Please use this identifier to cite or link to this item: http://elar.urfu.ru/handle/10995/112124
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dc.contributor.authorLasheen, E. S. R.en
dc.contributor.authorRashwan, M. A.en
dc.contributor.authorOsman, H.en
dc.contributor.authorAlamri, S.en
dc.contributor.authorKhandaker, M. U.en
dc.contributor.authorHanfi, M. Y.en
dc.date.accessioned2022-05-12T08:29:05Z-
dc.date.available2022-05-12T08:29:05Z-
dc.date.issued2021-
dc.identifier.citationRadiological Hazard Evaluation of Some Egyptian Magmatic Rocks Used as Ornamental Stone: Petrography and Natural Radioactivity / E. S. R. Lasheen, M. A. Rashwan, H. Osman et al. // Materials. — 2021. — Vol. 14. — Iss. 23. — 7290.en
dc.identifier.issn1996-1944-
dc.identifier.otherAll Open Access, Green3
dc.identifier.urihttp://elar.urfu.ru/handle/10995/112124-
dc.description.abstractMagmatic rocks represent one of the most significant rocks due to their abundance, durability and appearance; they can be used as ornamental stones in the construction of dwellings. The current study is concerned with the detailed petrography and natural radioactivity of seven magmatic rocks. All are commercial granitic rocks and are identified as black Aswan, Nero Aswan, white Halayeb, Karnak, Verdi, red Hurghada and red Aswan. Their respective mineralogical com-positions are classified as porpheritic granodiorite, granodiorite, tonalite, monzogranite, syenogran-ite, monzogranite and syenogranite. A total of nineteen samples were prepared from these seven rock types in order to assess their suitability as ornamental stones. Concentrations of 226Ra, 232Th and 40K radionuclides were measured using NaI (Tl) scintillation gamma-ray spectrometry. Among the studied magmatic rocks, white Halayeb had the lowest average values of226Ra (15.7 Bq/kg),232Th (4.71 Bq/kg) and40K (~292 Bq/kg), all below the UNSCEAR reported average world values or rec-ommended reference limits. In contrast, the other granitic rocks have higher values than the recom-mended limit. Except for the absorbed dose rate, other radiological hazard parameters including radium equivalent activity, annual effective dose equivalent, external, and internal hazard indices reflect that the White Halyeb rocks are favorable for use as ornamental stone in the construction of luxurious and high-demand residential buildings. © 2021 by the authors. Licensee MDPI, Basel, Switzerland.en
dc.description.sponsorshipFunding: We deeply acknowledge Taif University for supporting the researchers through Taif University Researchers Supporting Project number (TURSP-2020/287), Taif University, Taif, Saudi Arabia.en
dc.format.mimetypeapplication/pdfen
dc.language.isoenen
dc.publisherMDPIen1
dc.publisherMDPI AGen
dc.rightsinfo:eu-repo/semantics/openAccessen
dc.sourceMater.2
dc.sourceMaterialsen
dc.subjectGAMMA-RAY SPECTROMETERen
dc.subjectNATURAL RADIOACTIVITYen
dc.subjectORNAMENTAL STONEen
dc.subjectRADIOLOGICAL HAZARD INDICESen
dc.subjectGAMMA RAYSen
dc.subjectGRANITEen
dc.subjectHOUSINGen
dc.subjectRADIOACTIVITYen
dc.subjectRADIOMETRYen
dc.subjectSODIUM IODIDEen
dc.subjectGAMMA RAYS SPECTROMETERSen
dc.subjectGRANITIC ROCKSen
dc.subjectGRANODIORITEen
dc.subjectHAZARD INDICESen
dc.subjectMAGMATIC ROCKen
dc.subjectMONZOGRANITEen
dc.subjectNATURAL RADIOACTIVITYen
dc.subjectORNAMENTAL STONEen
dc.subjectRADIOLOGICAL HAZARDen
dc.subjectRADIOLOGICAL HAZARD INDEXen
dc.subjectGAMMA RAY SPECTROMETERSen
dc.titleRadiological Hazard Evaluation of Some Egyptian Magmatic Rocks Used as Ornamental Stone: Petrography and Natural Radioactivityen
dc.typeArticleen
dc.typeinfo:eu-repo/semantics/articleen
dc.typeinfo:eu-repo/semantics/publishedVersionen
dc.identifier.rsi47532387-
dc.identifier.doi10.3390/ma14237290-
dc.identifier.scopus85120308731-
local.contributor.employeeLasheen, E.S.R., Geology Department, Faculty of Science, Al-Azhar University, P.O. Box 11884, Cairo, Egypt; Rashwan, M.A., Geological Sciences Department, National Research Centre, 33 El Bohooth St. (Former El Tahrir St.), Dokki, P.O. Box 12622, Giza, Egypt; Osman, H., Department of Radiological Sciences, College of Applied Medical Sciences, Taif University, Taif, 21944, Saudi Arabia; Alamri, S., Department of Radiological Sciences, College of Applied Medical Sciences, Taif University, Taif, 21944, Saudi Arabia; Khandaker, M.U., Centre for Applied Physics and Radiation Technologies, School of Engineering and Technology, Sunway University, Bandar Sunway, 47500, Malaysia; Hanfi, M.Y., Institute of Physics and Technology, Ural Federal University, St. Mira, 19, Yekaterinburg, 620002, Russian Federation, Nuclear Materials Authority, Maadi, P.O. Box 530, Cairo, Egypten
local.issue23-
local.volume14-
dc.identifier.wos000735287400001-
local.contributor.departmentGeology Department, Faculty of Science, Al-Azhar University, P.O. Box 11884, Cairo, Egypt; Geological Sciences Department, National Research Centre, 33 El Bohooth St. (Former El Tahrir St.), Dokki, P.O. Box 12622, Giza, Egypt; Department of Radiological Sciences, College of Applied Medical Sciences, Taif University, Taif, 21944, Saudi Arabia; Centre for Applied Physics and Radiation Technologies, School of Engineering and Technology, Sunway University, Bandar Sunway, 47500, Malaysia; Institute of Physics and Technology, Ural Federal University, St. Mira, 19, Yekaterinburg, 620002, Russian Federation; Nuclear Materials Authority, Maadi, P.O. Box 530, Cairo, Egypten
local.identifier.pure29066694-
local.description.order7290-
local.identifier.eid2-s2.0-85120308731-
local.identifier.wosWOS:000735287400001-
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